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Atmosphere and Climate Change Chapter 13 Environmental Science Climate Weather – state of atmosphere at certain time Climate – long term conditions of atmosphere Factors determining climate Latitude Distance from the equator – north or south Low latitudes Night and day are the same length Temps high all year round High latitudes The sun is lower in the sky – less energy from sun Hours of daylight and temperature vary throughout the year What Factors Determine Climate? Atmospheric Circulation How wind is created The sun heats the ground and the air above it The warm air rises Cooler air moves in to replace it Global Circulation Patterns Near the equator Hot air pushes the cold air north or south Cold air sinks the further north or south it goes (less hot air present) What Factors Determine Climate? Prevailing Winds Winds that blow mostly 1 direction during the year Blow to the right in the Northern Hemisphere Blow to the left in the Southern Hemisphere Trade Winds Prevailing winds between 30° north and south Westerlies Prevailing winds between 30° and 60° north and south Polar Easterlies Prevailing winds between the poles and 60° north and south latitude Oceanic Circulation Patterns Ocean current movement Winds & Earth’s rotation El Niño (warm phase) Short-term change in location of warm and cold water masses in the Pacific Ocean More rainfall in the Southern US Drought in Indonesia and Australia La Niña (cold phase) Opposite of El Niño Pacific Decadal Oscillation (PDO) Topography Elevation affects the climate Height above sea level Higher up you go, the colder it is Mountain ranges affect the precipitation Rain on the west side of a mountain Dry on the east side of a mountain Seasonal changes due to tilt of the Earth Other Influences Sun The more sun, the more UV radiation The more UV rays, the more ozone The more ozone, the warmer the air Volcanoes Sulfur dioxide gas gets into the upper atmosphere Reacts with water vapor and dust Forms a layer of haze which blocks sun Can cause a decrease in the global temp. Assignment Page 334 Section 1 Review #1-4, 6 The Ozone Shield Ozone Layer Area in the stratosphere where ozone is highly concentrated Ozone is made of three oxygen molecules Absorbs most UV light from the sun UV light can damage genetic material & cause skin cancer Acts as a sunscreen for people Ozone hole Found in 1979 and is a thin layer of ozone Chemicals That Deplete the Ozone Layer Chlorofluorocarbons (CFCs) Nonpoisonous, nonflammable Used in refrigerator and air conditioner coolants Used as propellant in spray cans (paint, etc) When these chemicals get into the stratosphere, they break apart, absorb UV radiation and destroy ozone How Does the Ozone Hole Form? In Antarctica during the winter, winds of cold air surround the warm air The air becomes very cold Clouds with water and nitric acid form Polar Stratospheric Clouds CFCs are converted to chlorine In the spring, when the UV rays touch the chlorine, it splits and destroys ozone The destruction causes the ozone hole to form Can ozone replace itself? Ozone can be produced on the Earth’s surface as air pollution This ozone breaks down in the troposphere Therefore the ozone never reaches the stratosphere So, the answer is no. Ozone can not replace itself. Effects of Ozone Thinning on Animals and Plants UV light can kill phytoplankton This could disrupt the ocean food chains This could increase the amount of carbon dioxide in the atmosphere Damage to amphibian eggs Interferes with photosynthesis in plants Can lower crop yields Protecting the Ozone Layer In 1987, Canadian group met Agreed to use less CFCs In 1992, a conference in Denmark Countries agreed to eliminate CFCs by 2000 Companies developed CFC replacements No more aerosol cans Problem - CFC molecules remain in stratosphere for 60 – 120 years Assignment Page 338 Section 2 Review # 1-5 Global Warming The Greenhouse Effect Sunlight goes through the atmosphere Heats the Earth’s surface Some of the heat escapes into space The rest of the heat is absorbed by gases Greenhouse Gases Water vapor Carbon dioxide Chlorofluorocarbons Methane Nitrous oxide Carbon Dioxide Measuring the levels in the atmosphere Summer Levels are low due to photosynthesis Winter Levels are high due to dying grasses and fallen leaves releasing carbon into the air Most released greenhouse gas Power plants Cars Burning of rain forests for farmland How certain is global warming? Global warming Predicted increase in global temperature Scientists are unable to accurately predict the rate of global warming Too many variables involved They try to predict by using computer models They enter a large amount of data Consequences of Global Warming Melting ice and rising sea levels Erodes the beaches Coastal homes could be lost Coastal aquifers will become too salty Global weather patterns would change Warmer Earth means warmer oceans Increase in hurricanes More rain in areas – flooding problems Consequences of Global Warming Human Health Problems More heat-related deaths More respiratory problems Insect-borne diseases could spread Agriculture More droughts would occur Effects on Plants and Animals Could change the types of plant species Animals may change where they live Recent Findings Intergovernmental Panel on Climate Change (IPCC) – published report temp increased by 0.6°C in 20th century Predicts that human activity will make the temp and gases levels increase in 21st century Surface Kyoto Protocol Developed countries are to reduce emissions of carbon dioxide and other gases by 5 percent by 2012 Most developed countries agreed, US did not Reforestation projects Reduces carbon dioxide levels Assignment Section 3 Review Page 345 # 1-4, 6 Chapter 13 Review Pages 347-349 # 6-21, 24-27, 33 #36 – Write a paragraph to adequately answer this question.
